GeotechPE
Geotechnical
- Dec 25, 2005
- 18
Recently conducted UU triaxial test on remolded lean clay with sand at confining pressures of 7, 14 and 28 psi. Two specimens at each pressure (6 mohr cicles). Samples were remolded to 95 percent standard proctor at plus 2 percent of optimum MC. Initial saturation is about 75 percent. Samples were not backsaturated. Sheared at 1 percent per minute.
With UU tests on saturated clay I would expect phi = zero or very close to zero and C = some value. If I draw a strength envelope to the mohr circles (which fits the six circles very well) I get a phi = 21 degrees and c = 7 psi.
I am trying to explain the significant slope of the strengh envelope with the following:
1) Samples not saturated, therefore strength more resembles drained condition.
2) Too fast a shear rate for material or shear rate incorrectly set too high.
3) Sample overconsolidated by standard proctor remolding. I would expect this to occur to some degree but not to this magnitude.
Any one gone down this road before? Also does anyone have any references / papers on the amount of shear strength introduced by standard compaction test effort?
Thanks.
With UU tests on saturated clay I would expect phi = zero or very close to zero and C = some value. If I draw a strength envelope to the mohr circles (which fits the six circles very well) I get a phi = 21 degrees and c = 7 psi.
I am trying to explain the significant slope of the strengh envelope with the following:
1) Samples not saturated, therefore strength more resembles drained condition.
2) Too fast a shear rate for material or shear rate incorrectly set too high.
3) Sample overconsolidated by standard proctor remolding. I would expect this to occur to some degree but not to this magnitude.
Any one gone down this road before? Also does anyone have any references / papers on the amount of shear strength introduced by standard compaction test effort?
Thanks.